
sedimentary
Sandstone
Sedimentary Rock (Quartzose Sandstone)
Hardness: 6-7 on Mohs scale (due to quartz grains); Color: Varies widely including tan, brown, yellow, red, grey, pink, white; Luster: Dull to earthy; Crystal structure: Clastic texture composed of sand-sized mineral particles or rock fragments; Cleavage: None, breaks across grains.
- Hardness
- 6-7 on Mohs scale (due to quartz grains)
- Luster
- Dull to earthy
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Physical properties
Hardness: 6-7 on Mohs scale (due to quartz grains); Color: Varies widely including tan, brown, yellow, red, grey, pink, white; Luster: Dull to earthy; Crystal structure: Clastic texture composed of sand-sized mineral particles or rock fragments; Cleavage: None, breaks across grains.
Formation & geological history
Formed by the accumulation, compaction, and cementation of mineral particles or rock fragments (predominantly quartz) in environments such as deserts, rivers, beaches, and shallow marine areas over millions of years.
Uses & applications
Widely used in construction as building stone, dimension stone, paving material, and in the manufacturing of glass and abrasives.
Geological facts
Sandstone formations often create striking geological landmarks such as arches, canyons, and monuments due to differential weathering. Famous examples include the walls of the Grand Canyon and Petra in Jordan.
Field identification & locations
Identified in the field by its gritty texture like sandpaper and visible sand grains. Found worldwide in sedimentary basins, river valleys, and desert regions. Good indicator of ancient depositional environments.
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